Validation of OMI tropospheric NO2 column densities using direct-Sun mode Brewer measurements at NASA Goddard Space Flight Center

被引:99
作者
Wenig, M. O. [1 ,2 ]
Cede, A. M. [3 ]
Bucsela, E. J.
Celarier, E. A. [4 ]
Boersma, K. F. [5 ]
Veefkind, J. P. [6 ]
Brinksma, E. J. [2 ,6 ]
Gleason, J. F.
Herman, J. R.
机构
[1] City Univ Hong Kong, Dept Phys & Mat Sci, Kowloon, Hong Kong, Peoples R China
[2] Univ Maryland, NASA GSFC, Goddard Earth Sci & Technol Ctr, Baltimore, MD 21250 USA
[3] Univ Maryland, NASA GSFC, Earth System Sci Interdisciplinary Ctr, College Pk, MD 20740 USA
[4] SGT Inc, NASA GSFC, College Pk, MD 20770 USA
[5] Harvard Univ, Dept Atmospher Chem, Cambridge, MA 02138 USA
[6] Royal Netherlands Meteorol Inst, NL-3730 AE De Bilt, Netherlands
关键词
D O I
10.1029/2007JD008988
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
[1] This paper presents a comparison of NO2 data measured with the Ozone Monitoring Instrument (OMI) on board the EOS-AURA satellite with ground-based direct-Sun Brewer measurement data. Since its deployment in July 2004, OMI has provided more than 2 years of daily high-resolution (similar to 13 x 24 km 2 at nadir) NO2 vertical column density maps. We describe the retrieval, which includes an estimation of the stratospheric and tropospheric fraction of total NO2 columns, the air mass factor (AMF) correction based on detected tropospheric NO2 enhancements, and the generation of the gridded data product. We present a validation study of the gridded NO2 data set using data from a Brewer MK3 double monochromator in direct-Sun mode located at NASA Goddard Space Flight Center in Greenbelt, Maryland, USA. Monthly averages of coinciding measurements correlate well (r = 0.9) but OMI data are about 25% lower than the Brewer measurement data ( slope 0.75, intercept -0.38 x 10(15) molecules/cm(2)). We present a detailed uncertainty analysis for both ground and satellite data and discuss the possible reasons for the observed differences.
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页数:10
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